Advection of baroclinic eddies by depth mean flow

Observed zonal propagation speeds of nonlinear eddies, derived using an eddy tracking algorithm, are compared with the classical long Rossby wave speed, Doppler shifted by just the depth mean velocity, the latter obtained from annual mean hydrography and an ocean atlas. Despite neglecting any Dopple...

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Bibliographic Details
Published in:Geophysical Research Letters
Main Authors: Klocker, A, Marshall, DP
Format: Article in Journal/Newspaper
Language:English
Published: Amer Geophysical Union 2014
Subjects:
Earth Sciences
Oceanography
Physical Oceanography
Antarctic
The Antarctic
Antarc*
Online Access:https://doi.org/10.1002/2014GL060001
http://ecite.utas.edu.au/96089
Description
Summary:Observed zonal propagation speeds of nonlinear eddies, derived using an eddy tracking algorithm, are compared with the classical long Rossby wave speed, Doppler shifted by just the depth mean velocity, the latter obtained from annual mean hydrography and an ocean atlas. Despite neglecting any Doppler shift from baroclinic background flows, the correspondence between observed eddy propagation speeds and theoretical long Rossby wave phase speeds is improved in the Antarctic Circumpolar Current region, where both show eastward propagation at speeds of 13 cm s −1 , although the observed eastward eddy propagation speeds are systematically lower than the predicted Rossby wave phase speeds.

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